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As you saw in Chapter 8, when stress is applied uni- formly in all directions, it is called confining pressure (Figure 10.2A).
Confining pressure causes the spaces between mineral grains to close, producing more com- pact rocks that have greater densities.
Confining pressure versus three types of stresses Confining pressure A. changes the volume of a block of rock but not its general shape.
The major factors that influence the strength of a rock and how it will deform include temperature, confining pressure, rock type, and time.
The Role of Confining Pressure Recall from Chapter 8 that pressure, like temperature, increases with depth
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